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We analyzed the possibility of introducing a single stochastic scaling parameter a to describe the spatial variability of soil hydraulic properties, using the soil hydraulic properties of the Hamra field (Russo and Bresler 1981) and the Panache field (Nielsen, Biggar, and Erh 1973). In the traditional approach (Peck, Luxmoore, and Stolzy 1977; Russo and Bresler 1980; Warrick, Mullen, and Nielsen 1977), sets of scaling factors are estimated from the h(s) and K(s) functions. For "perfectly similar media," the two sets of a should be identical. Even though the sets of a in these studies were found to be correlated (table 2), they possessed different statistical properties, and were not identical. Results of structural analyses of the sets of a from the two fields suggested that the spatial structures of the two a-sets are quite distinct, reflecting the different spadal behavior of the h(θ) and the K(θ) functions. Moreover, there was poor correlation between the uncorrelated residuals of the a-sets, indicating that part of the high correlation between the a-sets found in earlier work must stem from the presence of an undetected drift and from correlation between nearby measurements. Under field conditions, the saturated hydraulic conductivity is controlled by the flow of water through large structural voids (macropores), which drain at very small negative values of water pressure. Because of this, we tried eliminating Ks by using relative hydraulic properties instead of the hydraulic properties themselves to estimate the scaling factor sets. For the Hamra field, for which we assumed that the hydraulic properties could be described by the model of Brooks and Corey (1964), we found the resultant sets of scaling factors to be highly correlated (R2 = 0.996) with the same spatial structure, but with slightly different variance. By examining the relationships between the two a-sets implied by the Brooks and Corey (1964) model we saw that (1) in general, both sets will be functions of the range of water saturation values used to estimate them, (2) the correlation between the two sets can be improved for media with broad pore-size distributions, and (3) the two sets will be identical if and only if the relative hydraulic conductivity function K,.(hr) is described by the deterministic function Kr(hr) = hy -2 ("strictly similar media"). This analysis suggests that, for media that are not well described by Kr = hr -2, a scaling factor would be required in addition to a in order to achieve agreement between scaled values of hr(θ) and Kr(θ) at all points. A general model Kr = hr -η was proposed, with η as a second stochastic scaling factor for media that do not obey the restrictive assumptions of macroscopic Miller similitude. In the Hamra field, this modified scaling procedure produced perfect agreement between the scaling hydraulic properties. In the Panache field, with values of η determined from linear regression analysis of the logarithmic transformations of Kr and h,., agreement was improved considerably between the scaled hydraulic properties as compared to the more restrictive scaling procedure. In contrast to the Hamra field, however, there remained some significant differences between the scaled properties. These differences may have been artifacts of the different methods used to estimate the hIs) and the K(s) functions for the Panache field. The results of our analysis suggest that in any transient transport problem involving both K(s) and h(s), the description of their spatial variability requires the use of at least three stochastic variates-Ks , α, and η-not a alone.
Agro-technology
(2001)
The leaf beetle Diabrotica virgifera virgifera (Coleoptera: Chrysomelidae), (D.v.v.), also called the western corn rootworm, is endemic to the New World and ranks among the top ten insect pests in worldwide grain production. D.v.v. causes annual damages of 1 billion US Dollars and is a notoriously difficult insect pest to control and manage, as entomological history of the past 50 years amply demonstrates (METCALF 1986). Considering recent emphasis on environmentally compatible and sustainable management strategies, entomologists and practitioners are encouraged to pay increased attention to novel approaches such as biotechnial methods which today are characterized by preferential use of signal compounds. Fortunately, both insect and plants provide a wide variety of such natural resources. In the case of D.v.v., sex pheromonesand plant kairomones as specific attractants and management tools are relatively well investigated through numerous contributions by GUSS et al. (1982), METCALF & METCALF (1992), METCALF (1994) and many recent publications on the advance and spread of D.v.v. within Europe (BERGER 1995-2004, HUMMEL 2003). Principle of MSD method: In this paper, the plant kairomone 4-methoxycinnamaldehyde (MCA), a specific attractant for D.v.v., is being used as a tool within the newly proposed "MSD" strategy. It combines a two pronge approach consisting as the well known mass trapping with the novel shielding and deflecting, called in short "diversion" and introduced here for the first time. An invisible “curtain” or “fence” of MCA vapor released from a MCA trap line establishes a behavioral barrier which the flying beetles cannot easily pass without being 1. either caught in one of the high capacity traps or 2. being diverted elsewhere. The net effect is a significant reduction in adult population density and oviposition within the MCA treated field as compared to an untreated control field. These effects can be experimentally measured by 1. adult beetle counts on maize plants, 2. by counts in independent monitoring traps baited with the D.v.v. sex pheromone, and 3. by egg counts taken in soil samples.
The Lake Chad Basin is a major geographical region in the central part of the Sudan zone of Africa. The northern parts, however, extend into the Sahel and the southern parts of the Sahara desert. It consists of an extensive shallow depression of about 1.536.000 km2 (600.000 miles2) of which about 10% lies in Nigeria. The greater part is shared between the three countries of Cameroon, Chad and Niger. Climatically and agriculturally, the Chad Basin lies within the dry or semi-arid zone of Nigeria. It is a marginal area which has experienced severe droughts and considerable environmental changes in recent years. The natural environment, its use and misuse, and the threat of life posed by environmental pollution dominate discussions on environmental change. But in addition to the natural or physical environment, there are other equally important 'environments' which deserve some attention in view of the role that they play in generating economic growth and in ensuring sustainable development which is the central issue in our concern about the environment. These other environments are the cultural environment, the political environment and the economic environment, both internal and external. In the Chad Basin, all these other environments, along with the natural environment have been greatly influenced by its land locked location in the heart of Africa.
The objective of this paper is to combine the environmental conception of the Kanuri with detailed findings of pedological and botanical field investigations. Interpretation of multitemporal satellite data and aerial photographs should provide land cover and land use information for an extended area. The area of investigation was outlined within the transitional zone from the clay plains to the sandy areas by interpretation of satellite images. The presented subset of a SPOT-XS-satellite image shows part of the Marte Local Government Area with its capital Old Marte in the north-eastern part of the image. The darker colours represent the clay plains while the lighter parts are related to the sandy areas. Almost half of the research area is covered by clay but all settlements are located on the slightly elevated sandy areas. Within these sandy areas different gray shades demonstrate the pattern of the rainy season farming area. Differences in colour within the clay plains are mainly due to variances in soil, water content and vegetation cover. In the north-eastern part of the image irrigation channels of the South Chad Irrigation Project are visible. The main attention, especially of the pedological and botanical research, was directed towards the south-western part of the subset in the vicinity of the villages of Wulwa, Dura, Kajere and Ngubdori.
The study investigates elements influencing agricultural development in villages of the hinterland of Gombe, Gombe State, Nigeria. It aims to discover changes in socio-economic and socio-cultural interactions that exist among household, region, nation and world market. Of special interests are rural households as well as wholesale markets where dynamic processes in the structure of agricultural enterprises and the individual reasons of innovations are recognisable. The final objective of the study is to analyse the agricultural sector in the investigated villages in time and space, by typifying rural households, there strategies of action in relation to different factors: for example, farmsize, cultivation techniques and marketing of agriculture products. The study is also interested in operational profits and costs of farms, income of households as well as expenditures, etc. Because of the fact that statistical work is still going on, it is only possible to present a small portion of the results. Namely, the change in cultivation and marketing of farm products with special emphasis on cash crops during the last 30 years.
The Nigerian agricultural sector deserves to be studied not less for the contribution of such knowledge to our understanding of the past, and present, but more for the usefulness of such knowledge in shaping the sector. The role that agriculture plays in Nigeria’s national economy since her independence may be determined by considering first, the changing structure of the national economy. As the national economy changes, also the role of agriculture. The observed structure at successive periods thus reveals the contribution that agriculture makes to the national economy. A total picture could also be presented through an examination of the contribution of agriculture to the gross domestic product GDP, over the years. It is also possible to add to the above presentation, the annual production of each agricultural crop over the period, or the productivity of the individual farmer as the years pass by. No doubt, the role of agriculture shall not remain static, for as deliberate efforts are made to develop the economy, the agricultural sector is also affected, although several endogenous factors also influence development within the sector. An emperical approach to the understanding of what is happening within the sector is to be prefered and such is documented in small scale studies conducted already by such scolars as FRICKE (1965), TIFFEN (1976) and MALCHAU (1999a+b).
The paper presents a short introduction to the environmental factors, e.g. climate, geology, relief forms and soils of the study area in the southern parts of the Gongola Basin. The study area covers the high mountain range of the Tangale-Waja Uplands and the adjacent pediplain, following in the north. It is asked if the natural factors enforced former inhabitants of the area to develop special land use techniques like field terracing to ensure the essential crop production under insufficient geoecological conditions.
In the culture of the Pero, Longuda and Tula People in the south-eastern part of Bauchi State, north-eastern Nigeria, terraces are found as traditional means to improve the environmental condition and to secure the survival of the people. To classify those terraces according to their form and function, the techniques and customs of their building and the traditional structures of their development they have to be compared in the context of their own culture. The paper gives a few examples showing that the importance of terraces for the historic and religious concepts of the Pero, Longuda and Tula People is expressed through a tight network of oral traditions, social and religious customs and structures of belief and explanation, which, once they were woven together, eventually build what a malam from Tula called a glue of inheritance, identity, integrity, continuity and security.
In Nigeria terrace agriculture can mainly be found in the so called "Middle Belt Economy" as FORDE (1946)1 coined this type which lies between the grain economy of males in the north and tuber cultivation of females in the south. The people - lacking a hierarchically social and territorial organisation - are called acephalous or segmentary societies. From the geographical point of view the Middle Belt is seen as a zone of transition. Because of the variability of the climate (sometimes it is too wet for grains, sometimes too dry for tubers) a strategy of mixed cropping enables the farmers to overcome these hazards. Their strategy can be seen in the frame of the game theory. A low population density and a lack of sufficient accessibility limited the innovation of cash crops at that time. The papers on the Tangale-Waja Region will reveal manifold facets of the culture and agriculture. In a first step we learn by the research of J. Heinrich that the natural environment is - from the genetic point of view - a prerequisite for the establishing of terraces, but it is still today an important provision to the modern farmers in their resettlement areas.
Obwohl Böden unzweifelhaft ein signifikanter Pool von organischem Kohlenstoff sind, ist ihre Bedeutung als potenzielle langfristige Senke für atmosphärischen Kohlenstoff keineswegs klar. Trotz bedeutender wissenschaftlicher Forschritte aus den letzten Jahren zur Klärung der Kohlenstoffdynamik in Böden gibt es nach wie vor offene Fragen insbesondere hinsichtlich der spezifischen geochemischen Mechanismen, die für die Stabilisierung organischen Kohlenstoffs in Böden verantwortlich sind. Vor diesem Hintergrund besteht ein wesentliches Ziel der vorliegenden Dissertation darin, in unterschiedlichen Bodentypen die Konzentration von organischem Kohlenstoff und Stickstoff sowie die mineralogische Zusammensetzung zu untersuchen, um Hinweise auf einen möglichen Einfluss der Tonmineralogie, der spezifischen Oberfläche und der Oxidkonzentration auf die Stabilisierung organischen Materials zu ermitteln. Die Ergebnisse sollen einen Beitrag dazu liefern, die Mechanismen der Fixierung organischer Substanz in Böden besser zu verstehen und das vorhandene Wissen hierüber zu erweitern. Hierzu wurden fünf verschiedene Bodenprofile aus Hessen mit unterschiedlicher mineralogischer Zusammensetzung untersucht. Um die Auswirkungen verschiedener physikalischer und geochemischer Faktoren auf den Gehalt organischer Substanz in den untersuchten Böden festzustellen, wurden folgende Parameter untersucht: -Tonmineralogie, -organische Kohlenstoff- und Stickstoff-Konzentrationen, -%-Kationensättigung, -spezifische Oberfläche, -dithionit- und oxalatlösliche Gehalte an Fe, Al und Mn. Anhand dieser Parameter wurden weiterführende statistische Analysen unter Verwendung der Statistiksoftware SPSS für Windows durchgeführt, um mögliche statistische Zusammenhänge aufzudecken, die für die Stabilisierung von organischem Kohlenstoff in den betrachteten Böden verantwortlich sind. Die im Rahmen der vorliegenden Dissertation ermittelten Ergebnisse zeigen, dass der Tonanteil und die Tonmineralogie der untersuchten Böden nur einen begrenzten Einfluss auf die Stabilisierung organischer Substanz haben. Weiterhin wird gezeigt, dass die in der Literatur propagierte Beziehung zwischen spezifischer Oberfläche und der Konzentration organischen Kohlenstoffs nicht auf alle Böden anwendbar ist. Die Ergebnisse deuten darauf hin, dass die Präsenz von amorphen Eisen- und Aluminiumoxiden der wichtigste Einflussfaktor für die Fixierung von organischem Material in den untersuchten Böden ist. Die größeren Konzentrationen von organischem Kohlenstoff in den kleinsten Fraktionen (Feinschluff und Ton) der Profile sind vor allem darauf zurückzuführen, dass Oxide ebenfalls in diesen Fraktionen aufzufinden sind. Tonminerale haben demnach eine sekundäre Bedeutung, indem sie Komplexe mit den Oxiden bilden, die zur Stabilisierung von organischer Substanz führen können. Insgesamt deuten die Ergebnisse daraufhin, dass Böden keine geeignete Senke für die langfristige Speicherung von organischem Kohlenstoff sind. Obwohl Mechanismen wie die Adsorption von organischer Substanz an Oxide die Stabilisierung organischen Materials unterstützen, scheinen diese nicht stark genug zu sein, um eine permanente Speicherung von organischem Kohlenstoff zu bewirken.